AA mass is suspended at the end of weightless wireof length cross sectional area&youngs modulas the period of oscillation for the am s.h.m. along the vertical direction is
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The atmosphere can be divided into layers based on its temperature, as shown in the figure below. These layers are the troposphere, the stratosphere, the mesosphere and the thermosphere. A further region, beginning about 500 km above the Earth's surface, is called the exosphere.
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